Reentry Layout - DJ05

Transcription

Reentry Layout - DJ05
GEORGE GONGORA/CALLER-TIMES
EARTH
Air & Space
December 2004/January 2005
NASA
How NASA can predict when space junk will fall in your back yard.
by James E. Oberg
December 2004/January 2005 Air & Space
NASA
O
The
Things
That
Fell to
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n January 15, 1995, a Japanese rocket took off
from Kagoshima, carrying a Russian-made satellite with German scientific instruments. The
mission’s purpose was to test materials processing techniques in microgravity and then return the samples to a landing zone in Australia.
But the launch vehicle swerved off course and headed
for the horizon. Ground controllers in Germany listened for
radio signals indicating that the satellite had reached a stable orbit, but they heard nothing. Without such confirmation, they eventually concluded it had fallen back to Earth.
Searching for the satellite was never considered since it
could have ended up almost anywhere, and all involved with
the mission assumed that the Russian spacecraft would never be seen again.
As it turned out, the heat-shielded landing capsule ended up in northern Ghana, near the town of Tamale, after the
satellite had limped around Earth twice in a lopsided orbit.
The capsule’s parachute had opened as planned, and as the
craft drifted down, it broadcast homing signals that nobody
picked up.
Villagers outside of Tamale witnessed the landing and
called the local schoolmaster. It was obvious to him that
the vehicle was a spacecraft and, given the Cyrillic characters on its side, probably of Russian origin. The schoolmaster organized a recovery team, who trucked the hardware to a storage
room in town.
Then he wrote to
officials in Accra
asking how to contact the satellite’s
owners.
Months later,
news of the space
object reached Geoffrey Perry, an
amateur satellite
tracker in England,
Nicholas Johnson (wearing tie)
who quickly realinterviews Barney Corey about an
ized it must be the
Ariane 5 nose cone found on a
lost Russian vehiTexas beach. Corey dug a hole
cle. He knew whom
behind his mobile home, intending
to call in the Gerto use his find as a hot tub, but the
man space procone was returned to its owners in
gram, and a few
France. In 1997, a fuel tank from a
months later,
Delta II launcher landed in Texas
staffers from the
(left). Four years later, a titanium
German embassy
motor casing from another Delta II
in Ghana showed
ended up in Saudi Arabia.
up in Tamale and
asked for their payload. Along with the capsule, the Germans were given a bill
for the storage fee, which they grudgingly paid.
Had the Germans known the capsule’s point of reentry
into the atmosphere, they could have avoided the storage
fee. Eight years later, another team desperately seeking another failed space vehicle knew its point of reentry. Using
models that can predict how space objects fall through
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The U.S. Air Force runs an observatory in Hawaii that
can track orbital debris.
FRANK RIZZO/ USAF
Earth’s atmosphere, this team was able to pinpoint not merely the continent, the country, and even the county where
something had fallen, but the likely pasture.
For weeks, searchers on foot had combed the ground in
east Texas, seeking pieces of the space shuttle Columbia,
which on February 1, 2003, had broken apart during reentry, killing all seven astronauts aboard. The location of
each fragment of the shattered shuttle was carefully documented, and then the parts were transported to a hangar at
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Air & Space
December 2004/January 2005
streaking through the sky from north to south. “I noticed
in the sky there was this big bright light, like a fire,” she told
a reporter from the Tulsa World newspaper. “I turned to
my friends to say look, and when I turned back it was coming towards us.” Then two sparks shot from the fireball and
disappeared over a building.
Later, when a slowly falling piece of charred woven material brushed Williams’ left shoulder and hit the ground
“with a metallic sound,” she concluded that there was a connection between the two events, especially since the next
day’s news was full of stories about “space junk” found on
the ground in Texas. A large stainless steel fuel tank, which
bore evidence of surface melting, had landed in the front
yard of a farmer near Georgetown, Texas, partially collapsing on impact. And outside the town of Seguin, a titanium pressurant sphere, undamaged except for some discoloration, had embedded itself halfway into a field.
Nicholas Johnson, chief scientist of the Orbital Debris
Program Office at Johnson Space Center, soon got word of
the discovered space debris. A few days later, he made the
drive from Houston to Georgetown, where he identified the
tank as having come from the one-ton second stage of a
Delta II rocket booster. The U.S. Space Command in Colorado Springs, Colorado, had been tracking the Delta II for
several days. Nine months earlier, it had launched a U.S.
Department of Defense payload. After the rocket stage’s orbit finally decayed, it had reentered the atmosphere around
3:30 a.m. over the south-central part of the country. The
reentry was seen by observers in Texas, Kansas, Missouri,
and Arkansas.
The collected orbital debris was shipped to the Johnson
Space Center. The fuel tank and the pressurant sphere found
in central Texas were obviously from the fireball. But investigators initially doubted that the piece of metal mesh
that had fallen on Lottie Williams was from the rocket, since
it had been recovered so far upstream of the bulk of the
Delta II’s debris.
At the Orbital Debris Program Office, Johnson is in charge
of NASA’s efforts to predict what sorts of space junk can
be expected to reach the ground after the natural decay of
objects’ orbits. Despite the fact that hundreds of fragments
of space objects have been found around the world and sent
to various government agencies, conventional wisdom is
that entering objects burn up. “Some launch companies until recently claimed in commercial launch license applications that spent stages totally burn up in the atmosphere,”
says Johnson. When the Russians remotely command the
supply vehicles that service the space station to reenter the
atmosphere, they claim that the vehicles “cease to exist,”
yet they choose to dump them over the far southern Pacific rather than over Russia—just in case.
According to William Ailor, director of the Center for Orbital and Reentry Debris Studies, between 100 and 200 large
(bigger than a breadbox) man-made objects reenter each
year. In 1999, Ailor has estimated, for example, that 212
tons of hardware hit the atmosphere, and a quarter of it,
about 42 tons, probably reached the surface. And during
the first 40 years of the Space Age, Ailor estimates that as
much as 1,400 tons of man-made material has reached the
December 2004/January 2005 Air & Space
TULSA WORLD
ARNOLD ENGINEERING DEVELOPMENT CENTER
Aerodynamicists tumbled a scale model of the space
shuttle’s external tank to simulate the stress of reentry.
Kennedy Space Center in Florida, where reconstruction efforts tried to help forensic engineers discover what had
gone so terribly wrong.
On March 18, a recovery team was sent to an area that
had already been searched; in fact, it had been marked “completed.” This time, though, the team was seeking one particular piece of hardware that had been aboard Columbia.
Knowing its size and weight, and the distribution of other
pieces already recovered, experts in reentry dynamics had
concluded that the 58-pound object—a VCR-size box containing potentially valuable flight data on the doomed mission—would lie in the already-searched area.
Sure enough, on a hillside near Hemphill, Texas, technicians found the Orbiter Experiment Recorder, embedded
several inches in the ground. It contained time-tagged measurements that were exactly what investigation teams needed to pinpoint the moment Columbia’s left wing had collapsed, an event that preceded the breakup of the vehicle.
The insights that led to the search team’s discovery had
been developed over many years of study at NASA’s Johnson Space Center in Houston, Texas, and an earlier instance
of spacecraft disintegration made the shuttle searchers confident that they were on the right track.
While out walking her dog with friends before sunrise on
January 22, 1997, a woman in Tulsa, Oklahoma, was hit by
a man-made object that fell out of the sky. Half an hour before, Lottie Williams had watched an impressive fireball
On January 22, 1997, Lottie Williams was grazed by a
slowly falling piece of mesh.
surface of Earth. He says, though, that worldwide, only
about 250 discoveries of authentic spacecraft pieces have
been reported because most pieces have landed in water.
For years, researchers had no reliable numerical models
to predict which pieces of a space vehicle would survive
entry and reach the ground intact. Estimates were made
“by guess and by golly,” says Johnson. But in the 1990s ITT
Systems in Alexandria, Virginia, developed a numerical model that took all known thermal processes into account in
order to predict the fate of entering objects. Around the
same time, a team of engineers from NASA and Lockheed
Martin worked jointly to create a numerical model called
Object Reentry Survival Analysis Tool (ORSAT).
Johnson and his team at NASA have found the ORSAT
program particularly helpful in understanding what happens to an object after the stress of deceleration causes it
to disintegrate. Once a satellite breaks up, for example, and
its individual components—often in the form of spheres,
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December 2004/January 2005 Air & Space
Air & Space
December 2004/January 2005
NASA
for the spacecraft of NASA’s Mercury manned space program. Or as space engineer Jim Davis says: “This is due to
the spacecraft performing work on the atmosphere like a
piston in a cylinder.”
The air molecules caught up in the shock wave created
by the incoming object can heat up to 11,000 degrees Fahrenheit, as hot as the surface of the sun. This heat
reaches the reentering
object mainly by conduction, as the superheated air molecules repeatedly strike its
surface. At higher reentry speeds—say, when
the U.S. Apollo manned
space capsules returned
from the moon at 25,000
mph—the compressioninduced shock wave becomes so hot that it
transfers much of its
heat into the reentering
object through direct
thermal radiation. And
at the speeds at which
meteors hit Earth’s atmosphere, up to 150,000
mph, nearly all of the
heat transfer is through
radiation.
Understanding how
objects break up and
scatter in the atmosphere is a relatively
new science for NASA,
but one with a wide
range of applications.
U.S. Forest Service
During space shuttle launchworkers (right) found the
es, for example, the exterbulk of debris from
nal fuel tank, which weighs
Columbia lying along a
44 tons empty, hits the at260-mile swath beginning
mosphere an hour or so afnear Fort Worth, Texas,
ter launch and breaks apart,
and extending across the
with metal fragments scatborder into Louisiana.
tering along a footprint in
the Atlantic Ocean. Mission
planners must place the entire footprint in a region that
sees little commercial sea and air traffic, and for some
launches, planners had difficulty finding a big enough dumping ground. But then a Lockheed Martin computer analysis
showed that the external tank was breaking up at a substantially lower altitude than first estimated and the pieces
were scattering over a correspondingly smaller area. Once
the computer prediction was confirmed by direct observation, shuttle mission planners had more leeway in calculating where the remnants of the tank could plunge.
Knowing what kinds of materials and structures are likely to survive entry and reach Earth intact also enables NASA
to calculate more reliable probabilities of property damage
and personal injury. In 2001, such calculations ended the
mission of the Compton Gamma Ray Observatory when it
was shown that the satellite’s heavy structural materials
presented a greater than 1-in-10,000 chance of harming property and people. The satellite had a gimpy control system,
so instead of waiting for it to fail and leave ground controllers with no means of directing the craft’s reentry, mission control dumped the
Just as computer models
satellite into the far southof reentry dynamics
ern Pacific Ocean while it
predicted, after Columbia
was still controllable.
broke apart, its flight data
Following the 2003
recorder (left) came down
Columbia disaster, the Cenon a hillside in the
ter for Orbital and Reentry
eastern Texas town of
Debris Studies became inHemphill.
volved in assessing the scatter pattern of fragments
from the shuttle. On
March 17, coincidentally just a day before
Columbia’s flight data
recorder was recovered,
CORDS director William
Ailor testified before a
public hearing of the
Columbia Accident Investigation Board in
Houston. Because the
Columbia accident investigators needed to
know whether the damage they saw on recovered fragments resulted from events that
happened earlier in the
shuttle’s flight (and that
may have led to the
disaster) or from
the stresses endured
during reentry, they
were interested in
learning how different materials
react to entering
Earth’s atmosphere.
The Columbia accident investigators
also wanted a way
to judge how thorough their search was by comparing the weight of recovered Columbia material to calculations of how much should
have reached the ground.
“For unprotected space hardware, the heating and loads
will gradually tear it apart,” Ailor explained to the investigators during the hearing. “The kinds of things that we’ve
seen that survive reentry are things that you would probably guess might—things like steel sometimes, glass, titanium, and then parts that are sheltered by other parts. One
Space Shuttle Debris Field
NASA
NASA
AP/WIDE WORLD PHOTOS
cylinders, and plates—are streaking in on their own, the
insulation. Because the mesh has no identifying marks or
reentries of the basic shapes are much easier to predict than
numbers, though, it cannot be proven to have come from a
those of the irregular shapes common to most intact satelparticular rocket. Still, the “circumstantial evidence is highlites. “Tumbling titanium spheres survive reentry totally inly convincing,” says Johnson, who points out that the mesh’s
tact,” says Johnson. Further, components with protuberlocation and time of landing are consistent with the 1997
ances are affected by aerodynamic drag differently than
Delta II reentry.
smooth components, with the protruding parts forming a
When an object reenters the atmosphere and breaks up,
“tail,” so that the front end of the object gets really roasted
the debris is scattered along a field, or footprint, with lighter
(some of NASA’s reports contain photographs of recovered
fragments landing near the “heel” of the footprint and heavspheres with burn holes opposite the protuberances).
ier objects traveling farther downrange toward the “toe”;
Johnson’s group has applied the ORSAT model to known
this explains why Williams’ mesh floated down in Oklaentry events, including the reentry and breakup of the nuhoma, far uprange of the heavier pieces that plowed into
clear-powered Russian satellite Kosmos 954, which rained
Texas. The ballistics characteristics of the heavy pieces also
radioactive debris over Canada on January 24, 1978. As the
ensure that they’ll travel at a higher velocity—and reach
ORSAT model predicted, Kosmos 954’s beryllium fuel rods
the ground sooner—than the lighter pieces.
became very hot during reentry. But the rods survived beLottie Williams wasn’t happy with these results, howevcause they were made of beryllium. “This is because of the
er. “I was thinking I had something celestial,” she told the
extremely high heat of fusion of beryllium,” says Johnson.
Tulsa World reporter. “And here I got something man-made.”
Steel and metals such as titanium and nickel share berylliThe ORSAT model can accurately predict entry heat loads
um’s ability to handle the heat, while aluminum and copon falling objects because it factors in the actual processper objects usually vaporize soon after breakup.
es at work. In contrast, the idea that air friction is the cause
Johnson is particularly
of reentry heat is persistent
proud of the ORSAT modbut misleading.
el’s results for debris from
Atmospheric entry heatthe Delta II rocket stage that
ing of man-made objects was
reentered over Texas in Janfirst noted in 1944, when
uary 1997. Using data such
Nazi Germany’s V-2 rocket
as size, weight, and compowarheads hit the atmosphere
sition for the fuel tank, presover London at about 6,000
surant sphere, and rocket
mph. As they reentered, comnozzle, the ORSAT model
pression-induced shock
indicated that all three pieces
waves heated the air ahead
would survive reentry, which
of the plunging warheads
they did. Additionally, the
enough to prematurely detORSAT program’s prediconate the explosives inside.
tion of the landing sites for
German engineers solved
all three pieces matched well
the problem by lining the
with the actual locations.
warheads with plywood to
Unlike the fuel tank and
serve as a heat shield.
the pressurant sphere, the
But after the Bell X-1 rockDelta II’s rocket nozzle is
etplane made its sound-barAuthorities in northwestern Canada had the unpleasant
made of the metal columbirier-breaking flight on Octask of gathering radioactive debris from Kosmos 954, a
um, which is mechanically
tober 14, 1947, confusion
Soviet nuclear-powered satellite that broke apart during
weak but can withstand high
began to set in about atmoreentry on January 24, 1978.
temperatures. The ORSAT
spheric heating. The X-1 and
model showed the rocket nozzle being heated quickly, then
other high-speed aircraft, such as the North American Xcooling quickly and eventually falling to the ground at a
15, which first flew in 1959, faced severe thermal environspeed of about 33 feet a second (compared to the impact
ments. Supersonic air rubbing across the aircraft’s outer
speed of the heavier tanks, 260 feet a second). As the nozskins created frictional heating, which had to be endured
zle approached the ground, it was already at air temperaor actively cooled. And from then on, the notion of atmoture. “Our research has shown that the material does surspheric heating was indelibly linked with air friction in mevive reentry,” wrote Johnson in a NASA report, “and that it
dia explanations and thus in the public mind.
‘floats’ down, landing approximately 30 minutes after the
But air friction has little to do with the process that heats
steel tank impact and 500–600 kilometers uprange.”
objects entering Earth’s atmosphere. The key source of the
What about the piece of mesh that hit Lottie Williams:
heating is compression: Air molecules in front of an inHad it also been shed from a Delta II? Williams has never
coming object can’t move out of the way fast enough, so
loaned the object to NASA, but she did send a fragment to
they pile up, or compress, which makes them very hot. The
the Center for Orbital and Reentry Debris Studies, which
air molecules get “aggravated,” as the late Max Faget liked
concluded that its composition is consistent with Delta II
to say when he explained how he invented the heat shield
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KSC/NASA
Forty percent of Columbia has been found and shipped to
Kennedy Space Center in Florida, where engineers
reconstructed the remains in an attempt to understand
the shuttle’s fate.
of the things about the reentry breakup process is that the
heating is like, in a sense, cooking an onion. You basically
start from the outside, and then as you heat the pieces up
to a point where the materials will fail, that will expose
some new materials. They’ll go through the same process
and the object can be broken apart. We do have objects that
are melted and shedded away, things like aluminum [and]
solar panels.
“For example, when an object comes off of a parent body,
it now experiences the air stream that exists there, and it
will respond based on its own characteristics. If you’ve got
a very lightweight piece that comes off of a heavier object
that’s coming through the atmosphere, it’s like throwing a
piece of paper out of a car. That will decelerate very quickly, and the same things happen even at Mach 20.”
Ailor went on to explain how timing and release conditions can affect survivability, both of particular significance
in the hunt for Columbia debris. “If an object comes out
late in the reentry, after being shielded for a portion of the
reentry, that means a lot of the energy has been taken out
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of that trajectory prior to that object’s release, and that object is more likely to survive,” he said. This shielding effect
explains why Columbia searchers found documents, videotape, cloth patches, and astronaut remains among the items
that made it to the ground.
Ailor estimated that anywhere from 10 to 40 percent of
a space object would actually survive reentry. The odds of
its being found, however, are much lower, even with the
models that CORDS has developed.
Careful study of the debris field from the Columbia accident helped improve the odds of success in that search.
As truckload after truckload of debris was gathered, NASA
engineers began to hope they could find particular pieces.
“We did analyze some specific components,” says Nicholas
Johnson. “Most already had been found, and we were asked
to go back and use our models to look at those locations.
We had very close agreement.”
Insights from such computer simulations and a reconstruction of the moments of Columbia’s breakup enabled
accident investigators to take the next step. With the Orbiter Experiment Recorder still missing, but with pieces
known to have been installed near it found, the region where
it ought to have fallen was carefully plotted, leading to its
recovery and its use to solve the more heartbreaking mystery of what destroyed the space shuttle.
Air & Space
December 2004/January 2005